ライフサイエンスコーパス: biogeochemistry

1 anisms that may strongly influence hyporheic biogeochemistry.

2 ems, and microbes drive most of its relevant biogeochemistry.

3 st affected by simultaneous changes in ocean biogeochemistry.

4 h water bodies and may strongly affect their biogeochemistry.

5 understorey lichen flora and changes in soil biogeochemistry.

6 omplementing other metrics of plant nutrient biogeochemistry.

7 ts increasing our understanding of organic P biogeochemistry.

8 oils is of vital importance to environmental biogeochemistry.

9 profound consequences for marine ecology and biogeochemistry.

10 l fluxes that have a global impact on marine biogeochemistry.

11 eded additional attention to global nitrogen biogeochemistry.

12 tical uncertainty in understanding hyporheic biogeochemistry.

13 ausing profound changes in planetary methane biogeochemistry.

14 crobe-host interactions, bioremediation, and biogeochemistry.

15 and therefore a central component of Earth's biogeochemistry.

16 ronutrient, iron plays a key role in oceanic biogeochemistry.

17 subsurface microbiota on carbon cycling and biogeochemistry.

18 tions for ecosystem services, processes, and biogeochemistry.

19 mework for linking ocean thermodynamics with biogeochemistry.

20 ture, but also impact hydrology, ecology and biogeochemistry.

21 ent for microbial community and arsenic (As) biogeochemistry.

22 cean linked to global impacts on climate and biogeochemistry.

23 and is thus of limited importance for ocean biogeochemistry.

24 ver-influenced water may influence estuarine biogeochemistry.

25 key role microbes play in modulating Earth's biogeochemistry.

26 al for risk assessments of ocean ecology and biogeochemistry.

27 Land Model (CLM4.5) with vertically-resolved biogeochemistry.

28 speciation, subsurface redox conditions, and biogeochemistry.

29 of dissolved organic S (DOS) in affecting S biogeochemistry.

30 e the role of animals in oxygen minimum zone biogeochemistry.

31 ommunity structure, biotic interactions, and biogeochemistry.

32 oxygenation event gave rise to modern marine biogeochemistry.

33 Saanich Inlet-a seasonally anoxic fjord with biogeochemistry analogous to oxygen minimum zones (OMZs)

34 tudes because of cold temperature effects on biogeochemistry and (ii) the N/P ratio increases with me

35 e as systems biology, microbiology, ecology, biogeochemistry and analytical chemistry are enhancing o

36 faunal group because of their role in marine biogeochemistry and as a food source for commercial fish

37 g of silicon transport with implications for biogeochemistry and bioinspired materials.

38 sformed into novel ecosystems with habitats, biogeochemistry and biological communities outside the n

39 d South Pacific have direct implications for biogeochemistry and carbon export in oligotrophic gyres.

40 and role of dust/Fe fertilization on marine biogeochemistry and climate.

41 e possible impact of that nutrient on marine biogeochemistry and climate.

42 roductivity plays a key role in global ocean biogeochemistry and climate.

43 ative understanding of relationships between biogeochemistry and climate.

44 lating with seasonal shifts in hydrology and biogeochemistry and clustering into three groups: winter

45 Microbial communities consume oxygen, alter biogeochemistry and compress habitat in aquatic ecosyste

46 nments and strongly influences both sediment biogeochemistry and contaminant fate.

47 ur results highlight the key roles of sulfur biogeochemistry and ecology in influencing estuarine fis

48 n boreal ecosystems with distinct hydrology, biogeochemistry and ecology that influence their carbon

49 onmental variable coupling physics to marine biogeochemistry and ecology.

50 global numerical model of ocean circulation, biogeochemistry and ecosystems suggests that Crocosphaer

51 ion of a high-resolution regional model with biogeochemistry and forecasts from NOAA's Climate Foreca

52 he atmosphere to the oceans, affecting ocean biogeochemistry and hence having feedback effects on cli

53 of many ecosystem processes including global biogeochemistry and horizontal gene transfer.

54 t ecosystem models describing hyporheic zone biogeochemistry and its influence over riverine ecosyste

55 cal link between contemporary aquatic carbon biogeochemistry and paleo-conditions in the watershed, a

56 ance because of its critical role in oceanic biogeochemistry and primary production.

57 amics in fundamental ways by controlling the biogeochemistry and productivity of the oceans.

58 face of oceans provides a link between ocean biogeochemistry and the atmospheric chemistry of the mar

59 e the relationship between sediment texture, biogeochemistry, and biological activity in the Columbia

60 ns at the intersection of marine ecology, Fe biogeochemistry, and both human and environmental health

61 and trophic structure, species composition, biogeochemistry, and climate, drawing on special feature

62 We examined a global ocean circulation, biogeochemistry, and ecosystem model that indicated a de

63 ignificantly influence oceanic productivity, biogeochemistry, and ecosystem processes.

64 lankton communities and affect productivity, biogeochemistry, and the efficacy of the biological pump

65 Marine viruses are critical drivers of ocean biogeochemistry, and their abundances vary spatiotempora

66 egimes and consequences for biodiversity and biogeochemistry are hotly debated.

67 unities have a strong impact on the regional biogeochemistry as evidenced by the low partial pressure

68 r light on potential fungal roles in U and P biogeochemistry as well as the application of these mech

69 data provide the first insights into uranium biogeochemistry at high pH and have significant implicat

70 the potential to affect carbon and nutrient biogeochemistry at local and possibly regional scales.

71 on deposition fluxes and their effect on the biogeochemistry at the ocean surface should be constrain

72 l hypoxic environments is relevant to global biogeochemistry because coastal hypoxia is increasing wo

73 rtant role in dissolved organic matter (DOM) biogeochemistry, but its relationship with the fluoresce

74 ale eddies may play a critical role in ocean biogeochemistry by increasing nutrient supply, primary p

75 acteria play an indispensable role in marine biogeochemistry by recycling dissolved organic matter.

76 , and the corresponding shifts in the lake's biogeochemistry, carbon cycling and food web structure.

77 ntially through their effects on belowground biogeochemistry--could either promote (i.e., for the 0.1

78 emistry, we apply ecological theory, aqueous biogeochemistry, DNA sequencing and ultra-high-resolutio

79 Therefore, changes in soil biogeochemistry driven by perturbations of climate may i

80 vide insights into ecosystem functioning and biogeochemistry during much of Earth's history.

81 Understanding sulfur (S) biogeochemistry, especially in those watersheds subject

82 from wetlands, suggest new frontiers in CH4 biogeochemistry, examine relationships between methanoge

83 notably in physiology and medicine, isotope biogeochemistry, forensic science, and palaeoclimatology

84 obtained a lake-sediment record of fire and biogeochemistry from a subalpine forest in Colorado, USA

85 The complexity of mercury (Hg) biogeochemistry has made it difficult to model surface w

86 nce of ocean thermodynamics, circulation and biogeochemistry in a global biochemistry and circulation

87 Hence, the biogeochemistry in bromeliad tanks remains poorly unders

88 Through modelling Se biogeochemistry in China we found that deposition and vo

89 ts the breadth of conditions influencing the biogeochemistry in shallow CO2-rich hydrothermal systems

90 pears of great interest especially in marine biogeochemistry, in carbon capture and storage and in ma

91 understanding of crop ecophysiology and soil biogeochemistry increases average yields for rice, wheat

92 Molecular phylogeny and biogeochemistry indicate that eukaryotes differentiated

93 Relevant to tropospheric biogeochemistry is irreversible transport from the strat

94 nity dynamics and their relationship to lake biogeochemistry is therefore essential to understanding

95 An important issue in mercury (Hg) biogeochemistry is to explore the influence of aqueous H

96 s, critical to our understanding of seawater biogeochemistry, its long-timescale geologic history is

97 lue assigned at the Max Planck Institute for Biogeochemistry Jena (MPI-Jena).

98 ing to be elucidated through a confluence of biogeochemistry, microbiology, ecology, molecular biolog

99 multidisciplinary collaborations, including biogeochemistry, microbiology, zoology, and plant scienc

100 s to peatland ecology, carbon sequestration, biogeochemistry, microbiome research, niche construction

101 Ocean General Circulation Model coupled to a biogeochemistry model for a 50% increase of atmospheric

102 using seafloor POC flux from a coupled ocean-biogeochemistry model, NEMO-MEDUSA, to investigate globa

103 e this issue, we coupled soil erosion into a biogeochemistry model, running at 1 km(2) resolution acr

104 state of Mato Grosso, using a process-based biogeochemistry model, the Terrestrial Ecosystems Model

105 fossil fuel CO2 emissions and a terrestrial biogeochemistry model, we produce the first estimate of

106 m the surface ocean for food, but most ocean biogeochemistry models predict global decreases in expor

107 Using linked economic and terrestrial biogeochemistry models, we examined direct and indirect

108 work for incorporating microbial activity in biogeochemistry models, which often base biomineralizati

109 trains the parameterization of process-based biogeochemistry models.

110 inadequately, incorporated into existing CH4 biogeochemistry models.

111 ifferent methodologies and spatial scales of biogeochemistry, molecular microbiology, and modeling, a

112 tween climate, the upper ocean, and deep-sea biogeochemistry need to be considered in determining the

113 , on average, > 61% of the variation in soil biogeochemistry occurred within plots, and the effects o

114 idered to dominate the microbial ecology and biogeochemistry of AMZs, recent environmental genomics a

115 geographic extent, relative importance, and biogeochemistry of AOM in 15 North American peatlands sp

116 ivotal functions in the trophic dynamics and biogeochemistry of aquatic ecosystems.

117 The biogeochemistry of arsenic (As) in sediments is regulate

118 ted CO2 ] on primary productivity and on the biogeochemistry of carbon (C), N, and phosphorus (P) acr

119 We describe the biogeochemistry of contrasting tributaries within its ce

120 also important contributors to the nitrogen biogeochemistry of coral reefs.

121 More broadly, the terrestrial biogeochemistry of earth system models must be criticall

122 tant consequences for the thermodynamics and biogeochemistry of ecosystems, both during the winter-to

123 be increasing and consequently impacting the biogeochemistry of glacial and proglacial ecosystems in

124 carbon (DOC) plays a fundamental role in the biogeochemistry of glacier ecosystems.

125 gen, and investigating processes shaping the biogeochemistry of global N reservoirs.

126 d geoscientists of the role FeOB play in the biogeochemistry of iron and other elements.

127 temporal changes in atmospheric CH4 and the biogeochemistry of its sources and sinks.

128 5 and 2010 were conducted to investigate the biogeochemistry of Lake Vida's brine system.

129 copepods are central to the productivity and biogeochemistry of marine ecosystems.

130 impact of increased nutrient loading on the biogeochemistry of mercury (Hg) is challenging to predic

131 steine (Cys) plays numerous key roles in the biogeochemistry of natural waters.

132 e impacting a nearby stream and altering the biogeochemistry of nearby ecosystems.

133 Reconstructing the original biogeochemistry of organic fossils requires quantifying

134 To address this gap, we examined the biogeochemistry of peat and dissolved organic matter (DO

135 The effect of phospholipid on the biogeochemistry of pyrite oxidation, which leads to acid

136 To more readily evaluate the complex biogeochemistry of selenium, a flow-through electrochemi

137 tabolic characteristics, geomicrobiology and biogeochemistry of the deep-sea piezophiles.

138 Microorganisms play an important role in the biogeochemistry of the ocean surface layer, but spatial

139 interactions influence the productivity and biogeochemistry of the ocean, yet they occur in miniscul

140 study demonstrates how dynamically sediment biogeochemistry of the Peru Margin has responded to glac

141 Microbial activities shape the biogeochemistry of the planet and macroorganism health.

142 efine the physical extent, heterogeneity and biogeochemistry of these NRZs, we investigated sediment

143 To better understand the biogeochemistry of these rocks, we performed microscale

144 Presently, little is known about the marine biogeochemistry of Ti and there is a distinct lack of oc

145 Biogeochemistry of uranium in wetlands plays important r

146 ay have a significant impact on the nitrogen biogeochemistry on Caribbean coral reefs by releasing la

147 lly to biological productivity-and hence, to biogeochemistry-on Earth.

148 Evaluation of lacustrine floc Fe, Pb, and Cd biogeochemistry over seasonal (summer, winter) and water

149 ng of the nature of high temperature methane biogeochemistry, providing insight into the physiology a

150 arch Community Earth System Model, version 1-Biogeochemistry, Representative Concentration Pathway 8.

151 model, a high-resolution regional model with biogeochemistry that simulates seasonal conditions in hi

152 here and shapes tropospheric composition and biogeochemistry through its effects on ozone, other oxid

153 ormation about dynamic iron and radionuclide biogeochemistry throughout realistic sediment redox cycl

154 terrestrial ecosystems significantly affects biogeochemistry throughout weathering profiles, the lowe

155 cy, we used recent developments in coccolith biogeochemistry to reconstruct equatorial Atlantic sea s

156 ases and the microbial population on uranium biogeochemistry under flow conditions.

157 , we predict microbial impacts on subsurface biogeochemistry via iron, sulfur, and complex carbon oxi

158 face water mixing, microbial communities and biogeochemistry, we apply ecological theory, aqueous bio

159 rols of seawater CO2-carbonate chemistry and biogeochemistry, which is essential to make accurate pre

160 obal coupled models of ocean circulation and biogeochemistry, which lack this regulatory mechanism an

161 his phenomenon as a biotic component of lead biogeochemistry, with additional consequences for microb

162 oplankton is one of the foundations of ocean biogeochemistry, with applications in algal physiology,